upper-level circulation

基本解釋

The evolution and enhancement of occluded frontal circulation in upper-level westerly jet and lower-level southerly jet are discussed by using a dry primitive equation model.
利用原始方程模式探討了高空西風(fēng)急流和低空南風(fēng)急流中錮囚鋒環(huán)流的演變和增強(qiáng)機(jī)制。
Through the analysis, it is shown that the Matsa s extratropical transition and the re-intensification are due to the intrusion of cold air from the upper-level trough into the typhoons circulation.
以一個(gè)在陸上長(zhǎng)久維持并最終演變成溫帶氣旋的登陸臺(tái)風(fēng)“麥莎”為研究對(duì)象，通過(guò)對(duì)其北上變性過(guò)程的分析發(fā)現(xiàn)，臺(tái)風(fēng)與中高緯西風(fēng)槽的相互作用使得冷空氣侵入是其變性加強(qiáng)的原因。